La Meseta Formation
| La Meseta Formation Stratigraphic range: Eocene |
|
|---|---|
| Type | Geological formation |
| Unit of | Seymour Island group.[1] |
| Underlies | Pleistocene glacial deposits |
| Overlies | Lopez de Bertodano Formation, Sobral Formation, Cross Valley Formation |
| Thickness | 557 m.[2] |
| Location | |
| Coordinates | Lua error in package.lua at line 80: module 'strict' not found..[3] |
The La Meseta Formation is a sedimentary sequence deposited during the Eocene.[2] The formation is found on Seymour Island, Antarctica.
La Meseta Formation lies unconformably on the Cretaceous Lopez de Bertodano Formation. It is an approximately 557 m thick sequence of poorly consolidated sandstones and siltstones. The depositional environment was probably coastal, deltaic or estuarine in character. The top of the sequence is an erosional unconformity to Pleistocene glacial gravels.[3][2] La Meseta Formation is just one of the sequences that make up the fill of the Late Jurassic to Paleogene James Ross Basin.[3]
Fossils
La Meseta Formation is extremely rich in fossils. It is famous for its penguin fossils, for example the two genera Archaeospheniscus and Palaeeudyptes. Other bird fossils include Dasornis, a genus of pseudotooth birds. There are also an abundance of trace fossils. Diplocraterion, Helminthopsis, Muensteria, Oichnus, Ophiomorpha, Skolithos, Teredolites and Zapfella have been described.[4] Over 35 species and 26 families of fish have been described from the Ypresian Cucullaea bed.[3]
List of bird fossils:
- Archaeospheniscus wimani
- Archaeospheniscus lopdelli
- Palaeeudyptes antarcticus
- Palaeeudyptes gunnari
- Palaeeudyptes klekowskii
References
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<references />, or <references group="..." />| Paleogene Period | ||
|---|---|---|
| Paleocene Epoch | Eocene Epoch | Oligocene Epoch |
| Danian | Selandian Thanetian |
Ypresian | Lutetian Bartonian |Priabonian |
Rupelian | Chattian |
